| Project/Area Number |
08454159
|
|---|
| Research Category |
Grant-in-Aid for Scientific Research (B)
|
| Allocation Type | Single-year Grants |
|---|
| Section | 一般 |
|---|
| Research Field |
Petrology/Mineralogy/Science of ore deposit
|
|---|
| Research Institution | The University of Tokushima |
|---|
Principal Investigator |
KOTO Kichiro Tokushima Univ., Fac.Integrated Arts & Sci., Prof., 総合科学部, 教授 (40029872)
|
|---|
| Co-Investigator(Kenkyū-buntansha) |
NUMAKO Chiya Tokushima Univ., Fac.Integrated Arts & Sci., Res.Assoc., 総合科学部, 助手 (80284280)
ISHIDA Keisuke Tokushima Univ., Fac.Integrated Arts & Sci., Prof., 総合科学部, 教授 (20116776)
|
|---|
| Project Period (FY) |
1996 – 1998
|
| Project Status |
Completed (Fiscal Year 1998)
|
| Budget Amount *help |
¥6,100,000 (Direct Cost: ¥6,100,000)
Fiscal Year 1998: ¥900,000 (Direct Cost: ¥900,000)
Fiscal Year 1997: ¥1,000,000 (Direct Cost: ¥1,000,000)
Fiscal Year 1996: ¥4,200,000 (Direct Cost: ¥4,200,000)
|
|---|
| Keywords | radiolaria / earth crust / alpha quartz / amorphous silica / microfossil / X-ray powder pattern / Sanbagawa / Jurassic period / X線回折プロファイル |
|---|
| Research Abstract |
This work has been done to elucidate diagenesis based on mineralogy and crystallography. Shell of microfossil radiolaria consists of amorphous silica and is known to crystallize in alpha quartz in diagenesis. A degree of crystallization is considered to have a close relation with diagenesis and can be estimated by crystallinity of alpha quartz of the shell. Crystallinity of the shell of radiolaria can
be determined by measuring the line width of X-ray powder pattern.
Specimens of radiolaria were obtained from mudstone, slate and chert of Jurassic period in Shikoku Sanbagawa belt. Amorphous silica of radiolaria in deep sea was used as standard. Every X-ray diffraction pattern of radiolaria shows unoriented powder pattern of alpha quartz. No diffraction pattern was observed from radiolaria in deep sea indicating amorphous silica. The line width becomes sharper in order of madstone, chert and slate. The results agree with the degree of diagenesis.
The degree of diagenesis was also estimated from particle size of alpha quartz of radiolaria shell. Specimens of radiolaria were obtained from sedimentary rocks in Eastern part of Shikoku. Particle size was observed under Scanning Electron Microscope. The particle sizes are distributed in the range between 2 and 15 micron depending on diagenesis.
Heat treatment of amorphous silica of radiolaria shell was carried out. Amorphous silica crystallized in alpha quartz at 600 and 700 ﾟC for 1 day.
In conclusion crystallinity and particle size of alpha quartz of radiolaria shell have close relations with the degree of diagenesis.
|
